Particularly dangerous situation (PDS) tornado watch issued, explosive supercells imminent

UPDATE:  7PM EDT  MONSTER TORNADO on LIVE WEBSTREAMING near Norman OK

STREAMING LINK

Update by Ryan Maue

A Particularly Dangerous Situation (PDS) tornado watch (#356) has just been issued for Central Oklahoma and North Central Texas including DFW and OKC.

DESTRUCTIVE TORNADOES...LARGE HAIL TO 3 INCHES IN DIAMETER...

THUNDERSTORM WIND GUSTS TO 70 MPH...AND DANGEROUS LIGHTNING ARE

POSSIBLE IN THESE AREAS.

Tornado likelihood is very high…  SPC Convective Outlook:

...CENTRAL/SOUTHERN PLAINS...

MORNING SATELLITE LOOPS SHOW A VIGOROUS AND PROGRESSIVE MID/UPPER

LEVEL SHORTWAVE TROUGH OVER THE SOUTHERN ROCKIES. THIS FEATURE IS

FORECAST TO ROTATE RAPIDLY EASTWARD INTO THE PLAINS AND BECOME

NEGATIVELY-TILTED THIS EVENING. LATEST TCC PROFILER DATA SHOWS 90+

KNOT FLOW AT 6KM...INDICATIVE OF THE MID/UPPER LEVEL WIND MAX THAT

WILL NOSE INTO THE PLAINS THIS EVENING. MEANWHILE... SOUTHERLY LOW

LEVEL WINDS WILL MAINTAIN UPPER 60S AND LOWER 70S DEWPOINTS ACROSS

MUCH OF NORTH TX...OK...AND SOUTHERN/CENTRAL KS. BY MID AFTERNOON

THE DRYLINE WILL EXTEND FROM WEST-CENTRAL KS INTO WESTERN OK AND

WESTERN NORTH TX. STRONG HEATING AND RICH MOISTURE...COUPLED WITH

NEAR DRY-ADIABATIC MID LEVEL LAPSE RATES...WILL YIELD AN EXTREMELY

UNSTABLE AIR MASS WITH MLCAPE VALUES OF 4000-4500 J/KG.

PRESENT INDICATIONS AND LATEST OPERATIONS/MESOSCALE MODEL GUIDANCE

INDICATE THAT DISCRETE SUPERCELL THUNDERSTORMS WILL FORM ALONG THE

KS/OK DRYLINE BY MID AFTERNOON AND MOVE RAPIDLY NORTHEASTWARD WITH A

RISK OF A FEW TORNADOES AND VERY LARGE HAIL. EARLY IN THE

EVENT...THE GREATEST TORNADO THREAT WILL BE OVER KS AS STORMS

INTERACT WITH PRE-EXISTING OUTFLOW BOUNDARY AND BACKED LOW LEVEL

WINDS.

AS THE AFTERNOON PROGRESSES...CONTINUED HEATING AND LARGE SCALE LIFT

DUE TO APPROACHING UPPER TROUGH MAY LEAD TO MULTIPLE ROUNDS OF

CONVECTIVE DEVELOPMENT ALONG THE DRYLINE. THESE STORMS WILL ALSO

TRACK ACROSS THE HIGH RISK AREA DURING THE EVENING. LOW LEVEL WINDS

WILL BE STRENGTHENING...WITH ALL CONDITIONS FAVORING THE

POTENTIAL FOR LONG-TRACKED STRONG/VIOLENT TORNADOES AND

VERY LARGE HAIL OVER PORTIONS OF NORTH TX...CENTRAL OK...AND

CENTRAL KS

Real-time Forecast Links:

Tornado Probability -- Outlook issued 1625z May 24, 2011

NCEP 4-km Radar Forecast from two versions of the WRF model (ARW and NMM cores):  48-hour animation initialized at 12:00z on May 24, 2011 (from Ryan Maue’s FSU website)

============================================================== UPDATE: I’ve added my own radar product for people to watch, click the image to animate it: If you want to track storms at the local level, download a free copy of StormPredator

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May 25, 2011 9:42 am

John Public says on May 24, 2011 at 8:37 pm:
The north end of the storm came through our area, with Tornado sirens blaring, and based on what we were seeing and hearing on the news we expected to see lots of damage from the storm. After getting out, we saw nothing. Based upon past storm warnings and storms (Tornadoes, 100-mph straight winds, heavy hail, and flooding) that have done lots of damage in our area, this storm for our area seems hyped in comparison.

John, we escaped any damaging hail, wind and ‘nadoes here as well … but that’s not to say there wasn’t weather just 5 miles away! Listening to the Collin County ARES net on 147.18 MHz there was ‘weather’ experienced by others, notably wind and hail and observed wall clouds. In Dallas and Tarrant counties proper experienced the fuller effects of hail and wind, and perhaps ‘nado action as well.
Now, a segue into a summary of reports from yesterday:
Map, 5-24-2011 Storm reports – http://oi53.tinypic.com/o6a9hz.jpg
Map and location/report data – http://www.spc.noaa.gov/climo/reports/110524_rpts.html
Thankfully, many of us escaped ‘the weather’; we should use the opportunity granted to assist those who were affected, because, surely, our ‘turn in the barrel’ will come about.
.

May 25, 2011 10:07 am

savethesharks says on May 24, 2011 at 9:03 pm:

THE FIRST THING THAT NEEDS TO GO: “Junk” computer-generated or doppler-indicated tornado (or even severe thunderstorm) “warnings”.

It is done so, using automated techniques, since, doing it manually could easily employ half a dozen individuals (analyzing the multiple ‘level plots’ generated by a WSR-88D RADAR, observing for differential velocities, taking into account storm movement, etc) and this would become tedious; this was once the case (doing it manually) using the old WSR-57 and WSR-74 ‘network’ (although not using Doppler; an operator (or several RADAR ops) was actually stationed at a console which had direct control over the WSR-57 RADAR dish and electronics and his job was to analyze, summarize and make observations of RADAR returns as they appeared – there was no storage available aside from the persistence of the phosphor used in the PPI CRT).
Early WSR-88D Tornado Detection Algorithm (TDA):
http://www.nssl.noaa.gov/divisions/warning/swat/tda.php

GOAL: To identify the locally intense circulations associated with tornadoes using Doppler radar data, provide useful guidance to warning operations, and provide at least a 10 minute lead time to tornadoes.
PHILOSOPHY: Identify ALL circulations within Doppler radar data (multiple scans) and distinguish between those which are tornadic and those which are non-tornadic.

This powerpoint (PPT) presentation explains how the WSR-88D (newer software) “Build 10 Tornado Detection Algorithm” works:
wx.db.erau.edu/faculty/mullerb/Wx365/Radar_nws/radarpt3.ppt

The Build 10 Tornadic Detection Algorithm ( TDA ) was developed at the National Severe Storms Laboratory (NSSL) and is designed to detect significant shear regions in the atmosphere. The WSR-88D TDA product in Build 10 displays more operationally pertinent information, and a new graphic symbol.
Performance of the TDA is better than TVS, with a higher probability of detection, some discrimination between tornadic and non-tornadic shear, and a requirement for gate- to-gate shear.

ADVANCED TORNADO DETECTION ALGORITHM USING SUPER-RESOLUTION
AND POLARIMETRIC DATA
ams.confex.com/ams/pdfpapers/155969.pdf

1. INTRODUCTION
The hook shape reflectivity feature has been documented as an indicator of tornadoes [Fujita, 1958], however more than half of the tornadoes have been reported
not associated with apparent hook signature. Tornado vortex signature (TVS) defined as the azimuthal velocity difference at a constant range is a parameter to quantify
the tornado feature based on pulsed Doppler radar observation [Burgess et al., 1975].
The basic idea of the current tornado detection algorithm (TDA) is to search for strong and localized azimuthal shear in the field of mean radial velocities [e.g., Crum and Alberty, 1993; Mitchell et al., 1998]. However, because of the smoothing effect caused by the radar resolution volume, the shear signature can be significantly degraded if the size of tornado is small and/or the tornado is located at far ranges [Brown and Lemon, 1976]. Recently, a neurofuzzy tornado detection algorithm (NFTDA) has been
developed by Wang et al. [2008] within atmospheric radar research center (ARRC) of the university of Oklahoma.
Tornado shear signature and tornado spectral signatures (TSS) are combined in this algorithm, and the performance shows significant improvement.

.

May 25, 2011 11:21 am

They still use human observation ground truth from Skywarn spotters to confirm what the radar is telling them. On many occasions when chasing storms NWS would call us and ask us what we were seeing, then moments after our report the severe warning would go out.
They need the ground truth to sort out some issues that the radar simply cannot tell them. Hail and heavy rain can sometimes be confused, and it really helps to get spotter confirmation that there is in fact a hail signature rather than heavy precipitation.
In addition, the radar cannot see all the way to the ground at a significant distance from the radar due to the curvature of the earth. They may be seeing mid level circulation at the lowest tilt sweep when the storm in 50-100 miles from the radar, and human observation confirming the existence of wall clouds and low level circulation is important to minimize over warning.
One of the problems is the general public has little appreciation of how local storm conditions can be. As a spotter I have dodged 2.5 inch hail on one side of a storm and just a couple miles away another spotter was sitting in bright sunshine and light winds. I have also been less than 1/2 mile from a large tornado and unable to even see it. I have had to drive around for a considerable time to find destructive hail swaths that are only a couple hundred yards wide and a 1/2 mile long. In open country, unless you know what to look for, you can drive right through a tornado path a few hours after it happened and never have a clue it had happened.
During the Last Chance tornado here in Colorado years ago, it put down several small funnels then formed a 1/4 mile wide wedge on the ground that tracked for several miles through farm country. It did remarkably light damage for the size of the storm simply because it failed to hit much. It slam dunked a few cattle killing them, tore up a farmers wind mill and made a grazing hit on the Chris Davis farm, pulled the roof off a barn (leaving a lantern hanging on a post peg untouched) tossing 25′ diameter grain bins a 1/4 of a mile, blowing all the windows out of 3 combines in the field, tried to pickup a household propane tank and spun it around a few times breaking the gas connections, leveled an old steel arch (Quonset hut style) garage, and carried a steel tank 12′ in diameter, and 20 ft long a 1/2 mile, and almost pulled the house off its foundation.
In spite of that long track and its size, it only took down about 3 power poles according to the rural electric crews I talked to that day. If you had not known a tornado had tracked through the area the day before, and did not come within site of the Chris Davis farm you never would have known it had happened except for a couple dead cattle in the fields.
When the wedge first formed, I was less than a mile away on the southwest side and only could see it for a few seconds before it rain wrapped and got swallowed up in the mist and rain.
Larry

SteveSadlov
May 25, 2011 11:50 am

Here’s what’s on tap:
=========================================
ON SUNDAY AN UPPER LOW IS FORECAST TO MOVE SOUTHWARD OVER NORTHERN CALIFORNIA BEFORE HEADING EAST TOWARDS THE GREAT BASIN. THERE ARE DIFFERENCES IN MODEL SOLUTIONS REGARDING THE WESTWARD EXTENT OF THIS LOW`S PATH…THUS WHETHER OR NOT THERE WILL BE ANY SHOWER CHANCES FOR OUR CWA. THE EARLIER RUN OF THE GFS TOOK THIS LOW FARTHER TO THE EAST FOR A COOL BUT DRY SOLUTION FOR OUR AREA… WHEREAS THE ECMWF HAS THE LOW CENTER ITSELF OVER SAN FRANCISCO BY SUNDAY MORNING. THIS WOULD WARRANT PUTTING SOME SHOWER CHANCES INTO OUR FORECAST FOR THAT DAY.
================================================
This one will hit the S. Plains early / mid next week, unless a good blocker builds north from the Gulf.

SteveSadlov
May 25, 2011 11:59 am

Sorry, forgot to mention that today’s front (e.g. the one I described bearing down on us yesterday) is also a good cold pool. Raining here right now (almost unheard of this late in the season).

Robert of Texas
May 25, 2011 7:20 pm

We had a big circulation pass over my house last night. It did some damage to the west (probably a tornado) but by the time it reached my area the circulation was becomming disorganized. Still, once the rain and hail had passed and I knew it was safe, I used this as an excellent opportunity to teach my kids about weather. We counted four small circulating cloud bulges before it had moved on.

rmark
May 25, 2011 8:35 pm

The Hinton – Langston tornado track in Oklahoma happily died down to F1 near Stillwater as it crossed north of our mobile home – the little wind turbine vent on top the storm cellar set up quite the buzz as the tornado passed by.

SteveSadlov
May 26, 2011 9:38 am

See the other thread. Yesterday’s cold pool produced tornadic events here in California.